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首页|期刊导航|大气科学学报|青藏高原观测对2020年长江中下游地区梅雨降水过程预报的影响

青藏高原观测对2020年长江中下游地区梅雨降水过程预报的影响

庄照荣 田伟红 陈雨潇 陈静

大气科学学报2025,Vol.48Issue(2):217-228,12.
大气科学学报2025,Vol.48Issue(2):217-228,12.DOI:10.13878/j.cnki.dqkxxb.20240506001

青藏高原观测对2020年长江中下游地区梅雨降水过程预报的影响

Impact of Qinghai-Xizang Plateau observations on the forecasting of Meiyu in the middle and lower reaches of the Yangtze River in 2020

庄照荣 1田伟红 1陈雨潇 2陈静1

作者信息

  • 1. 中国气象局地球系统数值预报中心,北京 100081||中国气象科学研究院灾害天气科学与技术全国重点实验室,北京 100081||中国气象局地球系统数值预报重点开放实验室,北京 100081
  • 2. 中国气象局地球系统数值预报中心,北京 100081||兰州大学大气科学学院,甘肃兰州 730000
  • 折叠

摘要

Abstract

The Qinghai-Xizang Plateau plays a significant role in influencing China's climate and weather pat-terns.Howe ver,the regional observation density is considerably lower than that of eastern China.Despite this spar-sity,observations from the Qinghai-Xizang Plateau can significantly affect weather forecasts for downstream areas,such as the middle and lower reaches of the Yangtze River.With advancements in the resolution of regional models,many operational forecasting systems in eastern China exclude the Qinghai-Xizang Plateau,leaving the impact of its observations on downstream forecast quality unclear.This study uses the CMA-MESO rapid updating cycle system to simulate the Meiyu weather event that occurred in early July 2020 in the middle and lower Yan-gtze River region.The study evaluates the influence of missing observations from the Qinghai-Xizang Plateau on the accuracy of forecasts for downstream weather systems.Results indicate that the absence of Qinghai-Xizang Plateau observations significantly degrades the 24-72-hour forecasts for surface 2-meter temperature and 10-meter wind fields in the middle and lower Yangtze River.It also negatively affects precipitation forecasts during the first three days.Analysis of the observational impact highlights that Qinghai-Xizang Plateau observations pri-marily influence the middle and lower Yangtze River region,with the largest variance in the 24-72-hour forecast signal occurring in these areas.Thus,improving forecast quality in the middle and lower Yangtze River requires accounting for upstream observational data from the Qinghai-Xizang Plateau and the spatiotemporal propagation of this.To enhance severe weather forecasting in eastern China,it is crucial to not only increase local observation infrastructure,such as radars and weather stations,but also to deploy additional radars and satellites in the Qinghai-Xizang Plateau.Incorporating three-dimensional observational profiles,such as soundings,and deploying mobile observation stations in regions prone to sudden localized heavy precipitation can significantly improve forecast quality.Additionally,to mitigate the limitations of finite-region models,approaches such as high-low reso-lution nesting,variable-resolution modeling,or blending analyses methods should be adopted to incorporate up-stream information.

关键词

青藏高原观测/梅雨期降水/三维变分/CMA-MESO/快速更新分析预报

Key words

the Qinghai-Xizang Plateau observations/Meiyu rainfall/3DVar/CMA-MESO/rapid refresh analysis and forecasting

引用本文复制引用

庄照荣,田伟红,陈雨潇,陈静..青藏高原观测对2020年长江中下游地区梅雨降水过程预报的影响[J].大气科学学报,2025,48(2):217-228,12.

基金项目

国家重点研发计划项目(2021YFC3000902 ()

2022YFC3004002) ()

国家自然科学基金项目(42375154) (42375154)

大气科学学报

OA北大核心

1674-7097

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